福建沿海风暴潮特征的分析

通过普查1960-2001年正面登陆我国东南沿海的台风,分析了福建沿海风暴潮的特征及其可能原因。台湾海峡特殊地形对福建沿海风暴潮的时空分布有明显影响,登陆岸段不同,台湾海峡对风暴潮的影响作用也不同,导致福建沿海风暴潮出现明显不同的分布和变化特征。当台风位于台湾海峡时,其大风区位置利范围不同,会影响福建沿海各地风暴增水的幅度。台风横穿台湾海峡时,易使福建沿海台风大风区中心岸段出现双增水峰现象,第一个增水峰出现在台风离开台湾岛进入台湾海峡后,第二个增水峰出现在台风登陆福建沿海前后。台风横穿台湾海峡有时会引起台湾海峡北部出现奇异增水现象,风暴潮与天文潮之间的相互作用可能是其重要原因。奇异增水峰往往出现在天文潮低潮附近,此时实际潮位并不高。     

Characteristics of water mass under the surface mixed layer in Tsushima Straits and the southwestern Japan Sea in autumn

Two different cold waters were found under the surface mixed layer in Tsushima Straits and the southwestern Japan Sea in autumn 2004. One is cold saline water with a low concentration of dissolved oxygen, and the other is cold less saline water with a high concentration of dissolved oxygen. The older saline water originates from the bottom of the East China Sea, strongly influenced by the Kuroshio water with high salinity. The bottom density in the eastern channel of the Tsushima Straits is coincident with that of the East China Sea in autumn, corresponding to the season when the cold saline water was frequently found in the Tsushima Straits. The newer less saline water originates from the front of Tsushima Warm Current between the Tsushima Warm Current water and the surface cold water in the Japan Sea. This water is formed by subduction above the isopycnal surface from the front of the Tsushima Warm Current.     

1994年9月16日台湾海峡7.3级地震静态库仑应力变化及断裂危险性初步研究

Using the focal mechanism solutions and slip distribution model data of the Taiwan Straits MS7.3 earthquake on September 16, 1994, we calculate the static Coulomb stress changes stemming from the earthquake. Based on the distribution of aftershocks and stress field, as well as the location of historical earthquakes, we analyze the Coulomb stress change triggered by the Taiwan Straits MS7.3 earthquake. The result shows that the static Coulomb stress change obtained by forward modeling based on the slip distribution model is quite consistent with the location of aftershocks in the areas far away from the epicenter. Ninety percent of aftershocks occurred in the stress increased areas. The Coulomb stress change is not entirely consistent with the distribution of aftershocks near the epicenter. It is found that Coulomb stress change can better reflect the aftershock distribution far away from the epicenter, while such corresponding relationship becomes quite complex near the epicenter. Through the calculation of the Coulomb stress change, we find that the stress increases in the southwest part of the Min-Yue (Fujian-Guangdong) coastal fault zone, which enhances the seismic activity. Therefore, it is deemed that the sea area between Nanpeng Island and Dongshan Island, where the Min-Yue coastal fault zone intersects with the NW-trending Shanghang-Dongshan fault, has a high seismic risk.     

A physical mechanism for the Atlantic–Pacific flow reversal in the early Miocene

Barotropic wind-driven steady ocean circulation patterns have been calculated for several different continental geometries during the Tertiary. Using a shallow-water model, flows are computed at 5-Ma intervals within the 60–20 Ma period, while keeping a fixed pattern of the wind-stress forcing. The most interesting changes in ocean circulation occur between 35 and 20 Ma, in which (i) the Antarctic Circumpolar Current appears because of the widening of Drake Passage, (ii) the Tethys Current disappears because of the closure of the Tethys Seaway and (iii) the transport through Panama Straits (between North and South America) reverses. The results are qualitatively in agreement with interpretations of changes in ocean surface currents drawn on the basis of proxy studies. A physical mechanism of the flow reversal through the Panama Straits is proposed based on a detailed analysis of the changes in wind-driven transport of both the Tethys Current and the Antarctic Circumpolar Current.     

Underway Measurement of Sea Surface Temperature and Salinity in the Taiwan Straits in August,1999

The distributional features of sea surface temperature and salinity(SST and SSS) in the Taiwan Straits have been analyzed using the SST and SSS underway measurements in August,1999.The characteristics of SST and SSS are summarized as foloows:There are several upwellings and diluted water in the Taiwan Straits.The upwellings are divided into two kinds:those along the western coast of the Taiwan Straits and those around the Taiwan Shoal.There are three sources of diluted water:diluted water of the Jiulongjiang River,diluted water of the Zhujiang River and diluted water of the Minjiang River.     

基于断块运动机制的台湾海峡两岸地震区划分及其地震关联性

地震区和地震带应为两种不同的划分方案，前者是以活动块体为对象进行分区的，后者是以活动断裂带为对象进行分带的，它们的划分目的和依据是不同的。以板块和断块运动学机制，以台湾大纵谷和福建滨海断裂为边界把台湾海峡及其两岸划分为台湾东部滨海地震区、台湾地震区和福建地震区。结果显示该地区地震特征具有较好的相关性，三个地震区和区内（台湾和福建地震区）均有自东向西地震活动强度逐渐减弱，区内活动幕持续时问趋于同步增长的特点。研究显示福建地震区M≥7．0级地震本区频度是最高的，认为该地震区受菲律宾海板块NW向运动影响的同时，受华南地块SE向运动的影响是明显的。     

解读海峡西岸经济区

2004年1月福建省委省政府提出建设海峡西岸经济区的发展战略.作者基于对中国宏观城市地理结构的研究,提出过一些类似的思想.在这篇文章里,作者以3个阶段的认识来解读海峡西岸经济区.早在1988年,作者在中国沿海6个都市连绵区的假设中,已经认为闽东南具有形成都市连绵区的潜在条件.在全国一级城市经济区的研究中发现,福建既不是长三角的紧密腹地,也不是珠三角的紧密腹地,而是它们二者共同的竞争腹地.在全国二级城市经济区框架中,福建省是一个相对完整的二级经济区.作者的研究和观点从理论和实证方面支持了海峡西岸经济区战略.最后对福建省未来的发展提出了几点建议.     

Developing direct shipping across the Taiwan Straits

Direct shipping across the Taiwan Straits has been restricted since 1949 for political reasons. Goods for cross-Straits trade must be transshipped via a third place, such as Hong Kong or a Japanese port. Since commercial activities across the Straits have become increasingly prosperous in recent years, the demand for direct shipping across the Straits is growing critically important and attracts great attention from all sectors. Businessmen who are involved in cross-Straits trade have criticized the higher costs and longer transit time of transshipment. This article explores possible solutions for shipping directly across the Straits. It discusses the mode of negotiation for settling the discrepancies in viewpoints between the two sides, and aims to provide a reference for governments from both sides.     

Bridges, Tunnels and Their Relationship to the Economic Development on Both Sides of Taiwan Strait

The construction of bridges and tunnels plays an important role in the social and economic development of cities and local regions. The planning of the bridge and tunnel across Taiwan Straits will have a positive effect on the economic development at each stage: preplanning, engineering construction, and the completion of the project. The two sides of Taiwan Straits have the advantage of a suitable location, consanguineous relationship, and appropriate geographic conditions. Currently, there are many economic and cultural communications between both sides of the Straits. The bridge and tunnel from Xiamen to Jinmen can be regarded as the beginning of the “golden link belt.” The total capability for sustainable development of Fujian Province ranks the sixth among 31 provinces in China, which will provide powerful support for the construction of the bridge and tunnel.     

基于区际经济联系的海峡西岸经济区空间整合研究

引入区域间相互作用的引力模型,以海峡西岸经济区作为研究对象,测算出城市间的经济联系强度,并用对应的航空、公路和铁路客运联系资料进行验证,得出海峡西岸经济区内部的主要联系方向以及省际的主要联系方向。研究结果表明,海峡西岸经济区内部的经济联系主要集中在东部的海峡西岸城市群;而海峡西岸经济区的省际经济联系方向仍然是长江三角洲和珠江三角洲地区,所得结论与实际基本吻合。